{"title":"对流层使无线电射线散焦","authors":"R. E. Wilkerson","doi":"10.6028/JRES.066D.047","DOIUrl":null,"url":null,"abstract":"When radio rays pass through t he atmosphere, they are defoc Llsed due to its presence. This effect is measu red by the divergence coefficient a nd general formulas are derived for D1, the divergence coefficient of t he direct ray, and D\" the divergence coefficient of the reflected rayassuming a smooth spherical earth . As examples, DI and Dz are shown for some typical cases with an \"exponential\" atmosphere (troposphere).","PeriodicalId":398550,"journal":{"name":"Journal of Research of the National Bureau of Standards, Section D: Radio Propagation","volume":"13 1","pages":"0"},"PeriodicalIF":0.0000,"publicationDate":"1962-07-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"1","resultStr":"{\"title\":\"Defocusing of radio rays by the troposphere\",\"authors\":\"R. E. Wilkerson\",\"doi\":\"10.6028/JRES.066D.047\",\"DOIUrl\":null,\"url\":null,\"abstract\":\"When radio rays pass through t he atmosphere, they are defoc Llsed due to its presence. This effect is measu red by the divergence coefficient a nd general formulas are derived for D1, the divergence coefficient of t he direct ray, and D\\\" the divergence coefficient of the reflected rayassuming a smooth spherical earth . As examples, DI and Dz are shown for some typical cases with an \\\"exponential\\\" atmosphere (troposphere).\",\"PeriodicalId\":398550,\"journal\":{\"name\":\"Journal of Research of the National Bureau of Standards, Section D: Radio Propagation\",\"volume\":\"13 1\",\"pages\":\"0\"},\"PeriodicalIF\":0.0000,\"publicationDate\":\"1962-07-01\",\"publicationTypes\":\"Journal Article\",\"fieldsOfStudy\":null,\"isOpenAccess\":false,\"openAccessPdf\":\"\",\"citationCount\":\"1\",\"resultStr\":null,\"platform\":\"Semanticscholar\",\"paperid\":null,\"PeriodicalName\":\"Journal of Research of the National Bureau of Standards, Section D: Radio Propagation\",\"FirstCategoryId\":\"1085\",\"ListUrlMain\":\"https://doi.org/10.6028/JRES.066D.047\",\"RegionNum\":0,\"RegionCategory\":null,\"ArticlePicture\":[],\"TitleCN\":null,\"AbstractTextCN\":null,\"PMCID\":null,\"EPubDate\":\"\",\"PubModel\":\"\",\"JCR\":\"\",\"JCRName\":\"\",\"Score\":null,\"Total\":0}","platform":"Semanticscholar","paperid":null,"PeriodicalName":"Journal of Research of the National Bureau of Standards, Section D: Radio Propagation","FirstCategoryId":"1085","ListUrlMain":"https://doi.org/10.6028/JRES.066D.047","RegionNum":0,"RegionCategory":null,"ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"","JCRName":"","Score":null,"Total":0}
When radio rays pass through t he atmosphere, they are defoc Llsed due to its presence. This effect is measu red by the divergence coefficient a nd general formulas are derived for D1, the divergence coefficient of t he direct ray, and D" the divergence coefficient of the reflected rayassuming a smooth spherical earth . As examples, DI and Dz are shown for some typical cases with an "exponential" atmosphere (troposphere).